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Ulexite Crystal USA Natural TV Stone Borate Mineral Specimen Collector Display Piece Genuine with Certificate of Authenticity

Original price was: £14.52.Current price is: £11.62.

(Actual as seen)

Only 1 left in stock

SKU: RP0533 Category:

Description

Natural Ulexite Mineral Specimen from the United States

This genuine Ulexite mineral specimen from the United States showcases the distinctive fibrous structure and optical properties that make ulexite one of the most fascinating minerals in the borate mineral group. Carefully selected for its natural structure and clarity of fibres, this specimen demonstrates the unique internal arrangement that gives ulexite its well-known visual characteristics.

The listing photographs display the exact specimen you will receive, allowing collectors and enthusiasts to clearly observe the natural fibrous texture, colour, and mineral form before purchase. Each specimen is unique due to natural variations in fibre density and mineral growth.

Mineral Identification and Scientific Classification

Ulexite is a hydrated sodium calcium borate mineral belonging to the borate mineral group. It is sometimes informally referred to as “TV Stone” due to the way its fibrous structure transmits light and images through the mineral.

Key mineralogical characteristics include:

  • Mineral Species: Ulexite

  • Chemical Formula: NaCaB₅O₆(OH)₆·5H₂O

  • Mineral Group: Borates

  • Crystal System: Triclinic

  • Mohs Hardness: 2.5

  • Lustre: Silky to vitreous

  • Transparency: Translucent

  • Crystal Habit: Fibrous aggregates forming masses or nodules

The mineral forms as densely packed bundles of microscopic fibres, which act as natural optical fibres capable of transmitting light through the stone.

Geological Formation of Ulexite

Ulexite typically forms within evaporite deposits, where mineral-rich water evaporates in arid environments and leaves behind borate minerals. These conditions commonly occur in dry lake beds or saline basin environments where dissolved boron, sodium, and calcium accumulate.

As evaporation progresses, borate minerals crystallise within sediment layers. Ulexite develops when the chemical balance of sodium, calcium, boron, and water produces hydrated borate crystals that grow together in fibrous structures.

Over time, these fibrous crystals accumulate in nodular masses within the evaporite sediments, forming the natural ulexite specimens found in mineral deposits.

Optical Properties and “TV Stone” Effect

Ulexite is widely known for its unique optical property known as fibre optic transmission. The parallel arrangement of the mineral’s microscopic fibres allows light to travel along their length.

When a flat surface of ulexite is placed over printed text or an image, the fibres can transmit that image from the bottom of the stone to the top surface. This optical behaviour is what gives ulexite the informal nickname “TV Stone.”

This effect occurs naturally due to the mineral’s fibrous internal structure and is a well-known demonstration used in mineralogy to illustrate natural optical fibre behaviour.

Colour and Surface Characteristics

Ulexite typically appears white to colourless, often displaying a silky or fibrous appearance on natural surfaces. When polished on one face, the mineral’s internal fibre structure becomes more visible, enhancing its optical transmission properties.

Common visual features of ulexite include:

  • Soft white to pale grey colour

  • Fibrous or silky surface texture

  • Light-transmitting internal fibre bundles

  • Rounded or nodular natural formations

The mineral’s fibrous structure can often be seen clearly when the specimen is viewed under strong light.

United States Borate Deposits

Many well-known ulexite specimens originate from borate-rich evaporite deposits in the western United States, particularly in regions with historical borax and borate mining activity. These deposits formed in ancient arid basins where mineral-rich lake waters repeatedly evaporated over long geological periods.

The geological conditions in these areas allowed borate minerals such as ulexite, colemanite, and borax to develop within the sediment layers.

Specimens recovered from these deposits are valued for their clarity of fibre structure and distinctive optical characteristics.

Mineral Collecting and Display

Ulexite is a popular mineral among collectors because of its unusual optical behaviour and distinctive fibrous crystal structure. Specimens such as this are commonly included in mineral collections and geological teaching displays due to their educational value.

Collectors appreciate ulexite for:

  • Unique fibre optic optical properties

  • Distinctive fibrous mineral structure

  • Geological connection to evaporite borate deposits

  • Scientific interest within mineralogy collections

This specimen is suitable for mineral collections, geological demonstrations, educational displays, or natural history cabinets.

Cultural and Traditional Associations

Throughout history, unusual minerals have appeared in decorative and symbolic contexts in different cultures. In some traditions, minerals displaying distinctive visual properties are traditionally associated with clarity and observation, interpretations based on cultural symbolism rather than scientific properties.

Authenticity and Certificate of Authenticity

This Ulexite mineral specimen from the United States is a genuine natural mineral. Each purchase includes a Certificate of Authenticity lifetime guarantee generic card, confirming that the specimen is a real mineral.

The photographs in the listing clearly show the exact piece you will receive, ensuring transparency for collectors and buyers.

Size and Specimen Details

Please refer to the listing photographs for full sizing and scale of the specimen. Images clearly show the fibrous mineral texture and overall shape so buyers can evaluate the piece before purchase.

This Ulexite mineral specimen from the U.S.A. represents a remarkable example of borate mineral formation and natural optical fibre behaviour, making it a distinctive addition to any mineral collection, geological display, or educational mineral cabinet.

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